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三重県伊勢市西部, 御荷鉾緑色岩類に伴う含アルカリ角閃石石英片岩
https://doi.org/10.14945/00000305
https://doi.org/10.14945/00000305e8a20e4c-5cff-461d-8dfe-38e2d87ac315
名前 / ファイル | ライセンス | アクション |
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KJ00000102645.pdf (685.6 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-01-25 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 三重県伊勢市西部, 御荷鉾緑色岩類に伴う含アルカリ角閃石石英片岩 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Alkali amphibole-bearing quartz schist in the Mikabu Greenstones, western Ise, Mie Prefecture, Japan | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | alkali amphibole-bearing quartz schist | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | amphibole zoning | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | winchite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Mikabu greenstone | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Mie Prefecture | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.14945/00000305 | |||||
ID登録タイプ | JaLC | |||||
アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
著者 |
坂野, 靖行
× 坂野, 靖行× 藤原, 隆雄 |
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書誌情報 |
ja : 静岡大学地球科学研究報告 巻 19, p. 1-6, 発行日 1993-07 |
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出版者 | ||||||
言語 | ja | |||||
出版者 | 静岡大学地球科学教室 | |||||
NDC | ||||||
主題Scheme | NDC | |||||
主題 | 458 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 三重県伊勢市西部の御荷鉾緑色岩類分布域から含アルカリ角閃石石英片岩が発見された。含アルカリ角閃石石英片岩は薄い層状(最大層厚30cm)を示し, 緑色岩と互層する。主要構成鉱物は角閃石, スティルプノメレーン, チタナイト, 石英および曹長石である。アルカリ角閃石はマグネシオリーベック閃石からクロス閃石に分類される。比較的粗粒なアルカリ角閃石(幅80μm程度)は累帯構造を示し, コアからリムに向かってFe^3^+/(Fe^3^+ + Al^v^i)が減少し(0.9→0.5), 最外縁部にウインチ閃石が存在する。またウインチ閃石は, マイクロブーディン構造を示すアルカリ角閃石の断裂部分にも存在する。アルカリ角閃石およびウインチ閃石はそれぞれ, 累進および後退変成作用時に形成されたと考えられる。 | |||||
言語 | ja | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Alkali amphibole-bearing quartz schist was found in the Mikabu Greenstones, western Ise, Mie Prefecture. The alkali amphibole-bearing quartz schist occurs as a thin layer (up to 30 cm wide), and is intercalated with greenstones. Major constituent minerals are amphibole, stilpnomelane, titanite, quartz and albite. Alkali amphibole is classified into magnesioriebeckite and crossite. Coarse amphibole (about 80/μm in width) is zoned with an alkali amphibole core and a winchite rim, and the alkali amphibole core has a compositional gradient such that Fe^3^+/(Fe^3^+ +A1^v^i) decreases (0.9 to 0.5) from the central part outward. Winchite also occurs between alkali amphibole grains which show microboudin structure. Alkali amphibole and winchite were considered to be formed during prograde and retrograde stages, respectively. | |||||
言語 | en | |||||
ISSN | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 03886298 | |||||
NII論文ID | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | NAID | |||||
関連識別子 | 110000413495 | |||||
NII書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00103190 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |